Japan Geoscience Union Meeting 2024

Presentation information

[J] Oral

O (Public ) » Public

[O-05] Stationary linear rain band: its generation mechanism, prediction and disaster mitigation

Sun. May 26, 2024 9:00 AM - 10:30 AM Exhibition Hall Special Setting (1) (Exhibition Hall 6, Makuhari Messe)

convener:Koji Sassa(Natural Science Cluster, Kochi University), Akira Wada(Tokyo Institute of Technology), Takahiro Sayama(Kyoto University), Yoshinori MIYACHI(Geological Survey of Japan, AIST), Chairperson:Koji Sassa(Natural Science Cluster, Kochi University)


9:42 AM - 10:02 AM

[O05-02] The impact of global warming on the "senjo-kousuitai"

★Invited Papers

*Shun-ichi Watanabe1, Hiroaki Kawase1, Yasutaka Hirokawa1, Yukiko Imada2,1, Masaya Nosaka1 (1.Meteorological Research Institute, 2.Atmosphere and Ocean Research Institute)

Keywords:Senjo-kousuitai, Global Warming, Large ensemble, Downscaling

In recent years, disasters caused by “senjo-kousuitai” have occurred every year in Japan. Whether global warming has an effect on the occurrence of senjo-kousuitai and whether the frequency and intensity of senjo-kousuitai will change with future warming is an important factor in assessing climate change risk and adaptation policies in Japan.
A senjo-kousuitai is relatively small in spatial scale and occurs infrequently. Large-scale ensemble calculations using high-resolution numerical models are required to evaluate such phenomena from a climatological viewpoint. In this study, a large-scale ensemble downscaling experiment was conducted using a regional climate model with a grid spacing of 5 km from the Database for Policy Decision-Making for Future Climate Change (d4PDF) to analyze the effects of global warming on the senjo-kousuitai. The results show that the number of senjo-kousuitai under future climates of 2 and 4 K rise are approximately 1.3 and 1.6 times larger than those under the present climate, respectively. The total precipitation in individual senjo-kousuitai is also projected to increase. The increase in water vapor associated with the rise in temperature is the main reason for this increase. On the other hand, the stabilization of stratification and the decrease in vertical shear may suppress the increase in senjo-kousuitai. Using the same system, we also analyzed the occurrence of senjo-kousuitai in 2023 and found that past warming had increased the probability of occurrence of senjo-kousuitai in 2023.